Research Article
On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results
Table 2
The EASMI calculated by the Guo and Han indices in the CTL and aerosol runs.
| Model | Guo index (CTL run) | Guo index (aerosol run) | Han index (CTL run) | Han index (aerosol run) |
| BCC-CSM1.1 | −31.41 | −30.93 | −4.82 | −5.03 | CanESM2 | −48.66 | −46.9 | −7.99 | −8.7 | CSIRO-Mk3.6.0 | −55.31 | −53.4 | −9.13 | −9.31 | FGOALS-s2 | −39.86 | −39.29 | −4.44 | −5.10 | GFDL-CM3 | Null | −28.84 | −9.40 | −10.8 | HadGEM2-A | −47.21 | −46.6 | −3.47 | −4.7 | IPSL-CM5A-LR | −31.07 | −30.80 | −13.50 | −13.40 | MIROC5 | −54.13 | −49.0 | −5.40 | −7.3 | MRI-CGCM3 | −21.10 | −20.68 | −13.98 | −14.4 | NorESM1-M | −44.02 | −42.74 | −5.62 | −6.9 | Ensemble results | −41.00 | −39.4 | −7.10 | −7.7 |
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Significant at the 0.10 level; significant at the 0.01 level; “Null” indicates that the SLP data in the GFDL-CM3 CTL run are missing.
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